Abstract
Five Co-Mg olivines (Co0.23Mg1.77SiO4, Co0.4 Mg1.6SiO4, Co0.92Mg1.08SiO4,Co1.45Mgo.55SiO4, and Co1.76Mg0.24SiO4) and Co2SiO4 have been systematically synthesized by a floating-zone method and investigated by X-ray diffraction methods in order to clarify the intracrystalline distribution of Co2+ and Mg2+ ions between two octahedral sites [M(l) and M(2)]. Anisotropic least-squares refinements of the structures including the cation occupancies indicate that Co2+ ions are strongly concentrated on the smaller M(l) octahedral sites over the Co-Mg olivine solid-solution series. The octahedral distortion for the M(l) site shows a larger increase with increasing Co2+ content, whereas that for the M(2) site shows a small increase. The intracrystalline distribution coefficient, KD = [MgM(2)CoM(2)]/[MgM(1)CoM(2)], attains a maximum of KD ⋍ 5.4 at about 50 mol% Co2SiO4.